Folding is the ductile deformation of rocks. This means that they change shape without fracturing. This can occur in some parts of the lithosphere if the conditions are correct (very low strain rates, high temperatures and/or high confining pressures).
Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.
The density of Earth's lithosphere is 2.5 gm/cm^3
The lithosphere is composed of oceanic crust (mostly basalt)
The lithosphere is divided into what we call tectonic plates.
The intertidal zone is not related to the oceanic lithosphere because it is located on the continental shelf.
Landforms on the lithosphere include mountain ranges, plateaus, plains, valleys, and canyons. These features are a result of tectonic processes such as folding, faulting, and volcanic activity shaping the Earth's surface over time.
How they are different: Folded rock forms when tersion makes the lithosphere break into normal faults. How they are the same: They both refer to the stress in the Earth.
The uppermost mantle and the crust makes the lithosphere.
The lithosphere is composed of the crust and uppermost hard, brittle mantle.
Lithosphere (apex)
The crust and the upper mantle are a geological part of the earth called the lithosphere. There are 2 parts of the lithosphere: the oceanic lithosphere, which is made up of land underneath water, and the continental lithosphere, which is the the part made of just land. The lithosphere lies on top of the asthenosphere. The lithosphere is made up of tectonic plates, which are pieces of land floating on the lithosphere.
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Oceanic lithosphere is dense enough to be forced down into the mantle. Continental lithosphere is not.
whats an antonyms for lithosphere
When two plates made of continental lithosphere collide, they can form mountain ranges due to the intense compressional forces generated at the collision boundary. The uplift and folding of rocks during the collision can give rise to large mountain systems like the Himalayas formed from the collision of the Indian Plate with the Eurasian Plate.
As odd as it is to think of things this way, continental lithosphere is more buoyant than oceanic lithosphere. The oceanic lithosphere is more dense.